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Published byEmory Dalton Modified over 9 years ago
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Motion of heavy particles settle down in response to an external force such as gravity, centrifugal force or electric forcegravitycentrifugal forceelectric force Rate of sedimentation depends on the strength of the field, masses and shapes of the particles Sedimentation Theory (a) Gravitational sedimentation (b) Centrifugal sedimentation -Sedimentation velocity -Sedimentation Equilibrium 2.2 Kinetic property Sedimentation
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(a) Gravitational SedimentationGravitational Sedimentation m F1F1 F2F2 F b (buoyancy) F g (gravity)
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(a) Gravitational Sedimentation m F 1 = fV g F 2 = mg(1 - 2 / 1 ) At equilibrium : fV g = mg(1 - 2 / 1 ) m = fV g g(1 - 2 / 1 ) M = fN A V g g(1 - 2 / 1 ) 1 = density of particle 2 = density of medium F1F1 F2F2
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(b) Centrifugal Sedimentation sedimentation velocity sedimentation equilibrium = angular velocity (rpm)
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b.1 Sedimentation velocity an analytical ultracentrifugation method that measures the rate at which molecules move in response to centrifugal force generated in a centrifuge. This sedimentation rate provides information about both the molecular mass and the shape of molecules. In some cases this technique can also measure diffusion coefficients (D).
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b.1 Sedimentation velocity F1F1 F 1 = fV = f(dr/dt) F 2 = m 2 r (1 - 2 / 1 ) At equilibrium : f(dr/dt) = m 2 r (1 - 2 / 1 ) M = sfN A = sRT (1 - 2 / 1 ) D (1 - 2 / 1 ) S = (dr/dt) = m (1 - 2 / 1 ) 2 r f r F2F2 s = sedimentation coefficient (Svedberg, 1Sv=10 -13 s) ~ 80,000 rpm
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b.2 Sedimentation equlibrium M = 2RT ln (C 2 /C 1 ) (1 - 2 / 1 ) 2 (r 2 2 -r 1 2 ) ~ 10,000 rpm =
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Assignment-3 Group Presentation Comparing to sedimentation G1 : precipitation, aggregation G2 : coagulation, flocculation (10 students per group) (5 min)
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3. Optical property A colloidal system contains particles that affect a light beam by scattering and absorption. If the particles are of a size comparable to the wavelength ( ) of light or larger, they scatter or absorb light independently. The same thing happens if they are separated by distances comparable to or greater than the wavelength ( ) of light.
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3. Common Optical phenomena the interaction of light from the sun or moon with the atmosphere, clouds, water, or dust and other particulates
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Assignment-4 Group Presentation G3 : Rayleigh Scattering G4 : Raman Scattering G5 : Mie Scattering G6 : Bragg Scattering (10 students per group) (5 min)
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